Sentences with phrase «high latitudes as»

The significance is that one can readily observe the extent and intensity of the cold air covering the northern high latitudes as a whole at the time and date of each map.
in response to the increase of atmospheric carbon dioxide, the excess of precipitation over evaporation increases, and surface salinity is reduced in high latitudes as noted in section 8.
But Alaska had the aurora borealis, the natural display of colored lights created at high latitudes as charged particles hit the atmosphere.
As the effects of climate change play out, it is expected to expand its stomping ground into higher latitudes as temperatures rise (Bulletin of Entomological Research, doi.org/b6jjzd).
To date, research focusing on the connection between these two threats has primarily focused on the idea that species from lower latitudes, which typically experience warmer temperatures than those in higher latitude ecosystems, will perform better at higher latitudes as temperatures warm.
So one can rationalize the result that the centers of action for internal variability in the oceans migrate poleward from the tropics and subtropics to higher latitudes as one moves to lower frequencies.

Not exact matches

As the US military's attention shifts back to great - power competition, particular focus is being paid to the potential for conflict in the extreme conditions found at northern latitudes and higher elevations.
Black is the original or «normal» skin color for humans — lighter skin colors evolved in the last few tens of thousands of years as populations adapted to higher latitudes.
High mountains and latitudes were once thought far too bleak for ancient humans, but as icy patches melt they are revealing a rich world of human history
Examining the radiation balance as a function of latitude, we see that tropical regions have a radiation surplus; the deficit over the higher latitudes peaks at the poles.
We might expect that as ocean temperatures warm at higher latitudes more tropical storms could persist farther north.
While permafrost thawing or boreal wetlands in high latitudes have values of about -60 ‰, tropical wetlands — such as would be found in those regions — have slightly less negative values, about -52 ‰.
It also uses a low - resolution ocean model that doesn't include key currents that transfer heat to higher latitudes, such as the Gulf Stream.
Previous work by Hook using satellite data indicated that many lake temperatures were warming faster than air temperature and that the greatest warming was observed at high latitudes, as seen in other climate warming studies.
Based on how intact a given ecosystem is as well as how much climate change it is expected to endure, they suggest that the high latitudes and high altitudes are likely to see the most change.
The news isn't all bad: As the world's prime grape - growing regions shift to higher, cooler latitudes, today's marginal areas will become sweet spots.
This is especially true for lakes at high latitudes that are covered in ice each winter but may see less ice as temperatures rise.
In this pattern, warm waters flow northward from the tropics, then cool and become saltier and denser as they reach higher latitudes.
«At the higher latitudes of Great Britain, Scandinavia and the Baltic States, as well as Northern Germany and France, very little UVB light reaches the Earth, and it's the key wavelength required by the skin for vitamin D generation,» Elias said.
Dozens of studies have already demonstrated that species are shifting their geographic ranges over time as the climate warms, towards cooler habitats at higher elevations and latitudes.
A group of scientists and representatives of indigenous Arctic communities has identified areas around the Arctic Ocean that they consider especially worthy of consideration for protection as sea ice recedes and industry poises to enter the increasingly accessible high northern latitudes.
Aurora borealis is usually seen in high northern latitudes — this photograph was taken in 2004 in Langhus, Norway — but it has been seen far south as Arizona, Texas, and San Diego.
For example, in higher latitudes such as northern Canada and Greenland, coastal waters usually act as carbon sinks, absorbing excess carbon dioxide from the atmosphere.
They are commonly found on the surface of rocks on Earth and can survive in extreme conditions such as high mountains latitudes.
All of which means that new regions will be at risk for stronger storms as tropical cyclones spread to higher latitudes.
As temperatures around the world rise, species are being pushed to higher latitudes and altitudes to find places where they can live.
The extraordinary cold spell was probably strengthened and lengthened by the resulting increase in sea ice at high latitudes, as well as an unusually low number of sunspots in the middle of the 7th century.
It needs to be clarified here, that it is hypothetically possible to get more snowfall and snowpack in a globally warming world (at least for a while), due to increased precipitation (which is predicted in a warming world, esp for the higher latitudes) coming down as snow.
However, ENSO also increased the mean and variability of MHW duration in the northeast Pacific Ocean (Supplementary Fig. 1E, F), the variability of intensity off Western Australia and California (Supplementary Fig. 1D) and the variability of frequency over much of the Tropics in all ocean basins as well as the mid - and high - latitudes in the Pacific Ocean (Supplementary Fig. 1B).
al, (June, 2005): [During the Paleocene - Eocene thermal maximum (PETM), sea surface temperature (SST) rose by 5 Deg C in the tropics and as much as 9 Deg C at high latitudes, whereas bottom - waters temperatures increased 4 to 5 C.
As Cassini soared above high northern latitudes on Saturn's moon Dione, the spacecraft looked down at a region near the day - night boundary.
Projected number of fish species in high latitudes under business - as - usual greenhouse gas emissions.
With higher precipitation, portions of this snow may not melt during the summer and so glacial ice can form at lower altitudes and more southerly latitudes, reducing the temperatures over land by increased albedo as noted above.
In circunstances where these factors combine — planting trees as carbon offsets above the lcal tree line at high latitudes, modeling indicates that the radiative forcing impact can outwigh the benefits of carbon sequestration = cf
There just isn't much ice left, and what is left would be extremely difficult to melt, as most of it is located at high latitudes around the poles which are mostly dark 6 months out of the year with way below freezing temperatures.
Due to different regional temperature responses from the tropics to high latitudes, as well as between hemispheres, commonly used concepts such as «mid-Holocene thermal optimum», «altithermal», etc. are not globally relevant and should only be applied in a well - articulated regional context.
Cosmic dust in the high latitudes of the Milky Way could account for the entire swirl pattern that had been presented as proof of a leading Big Bang theory, according to a new data analysis from the Planck satellite.
In these high latitudes, temperatures are predicted to warm so fast and to such a degree so as to cause unprecedented melting of ice that even the most ardent of climate skeptics would be forced to concede the verity of global warming theory.
As you can see, things get especially warm, relative to what the Earth is used to, as you enter the very high latitudeAs you can see, things get especially warm, relative to what the Earth is used to, as you enter the very high latitudeas you enter the very high latitudes:
As the warm water reaches high North Atlantic latitudes, it gives up heat and moisture to the atmosphere, leaving cold, salty, dense water that sinks to the ocean floor.
With the more recent understandings of the ways reduced sunlight affects many people, bringing to our attention extreme reactions, such as SAD (Seasonal Affective Disorder) and high rates of suicide in latitudes of Earth that have fewer annual days / hours of sunlight, we now have support for Lessing's «far - fetched» propositions.
The second possibility, as feedback to higher sea surface temperatures, seems also more sensitive for solar in the tropics than for GHGs in the higher latitudes...
This results in the stable boundary layer being a common feature, particularly in the winter at middle and high latitudes (e.g. such as the Grand Valley of Colorado).
The paragraph in the OP you quote from as well as the one above it in full are saying that the ice age cycles result from the Earth's changing orbit round the sun which creates changes in the «incoming solar radiation (insolation) at high latitudes» (Roe (2006) PDF).
I was thinking instead perhaps more easily controlled polar - orbit satellites might be used, which would rotate with some fixed ratio to their orbital period, casting greater shadows at higher latitudes... or some other arrangment... for a targetted offset polar amplification of AGW especially and in particular perhaps avoiding the reduction in precipitation that can be caused by SW - radiation - based «GE» (although aerosols that actually absorb some SW in the troposphere while shielding the surface would have the worst effect in that way, I'd think)... strategic distribution of solar shading has been suggested with precipitation effects in mind, such as here... sorry, I don't have the link (I'm sure I saved it, just as Steve Fish would suggest — but where?).
«Yes, sea ice seems to behaving as the consensus of the climate models have been projecting — more rapid and larger response in the northern high latitudes than anywhere else, flat to possible increase in [southern hemisphere] sea ice as warming takes hold,» he wrote.
As the area / volume ratio for the NH parts of the oceans is practically the same as for the SH, the surface heating (W / m2) must be larger in the NH parts, within the constraints of heat exchange via ocean and air currents (and partly by the difference in warming area in the tropics vs. the cooling areas in the higher latitudes).As the area / volume ratio for the NH parts of the oceans is practically the same as for the SH, the surface heating (W / m2) must be larger in the NH parts, within the constraints of heat exchange via ocean and air currents (and partly by the difference in warming area in the tropics vs. the cooling areas in the higher latitudes).as for the SH, the surface heating (W / m2) must be larger in the NH parts, within the constraints of heat exchange via ocean and air currents (and partly by the difference in warming area in the tropics vs. the cooling areas in the higher latitudes)...
Also, if you look at Table T2 in this paper, you will see that ocean sea surface heat storage 0 - 700m from 1955 - 2003 (in W / m2) is always higher at northern latitudes than the corresponding southern latitudes in every case, even with the extensive Southern Ocean warming as noted by Gavin responding to # 18.
In the tropics, simple thermodynamics (as covered in many undergraduate meteorology courses) dictates that it should actually warm faster, up to about 1.8 times faster by the time you get to 12 km or so; at higher latitudes this ratio is affected by other factors and decreases, but does not fall very far below 1.
This would actually not be true at sufficiently high latitudes in the winter hemisphere, except that some circulation in the upper atmosphere is driven by kinetic energy generated within the troposphere (small amount of energy involved) which, so far as I know, doesn't result in much of a global time average non-radiative energy flux above the tropopause, but it does have important regional effects, and the result is that the top of the stratosphere is warmer than the tropopause at all latitudes in all seasons so far as I know.
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